Movatterモバイル変換


[0]ホーム

URL:


Jump to content
WikipediaThe Free Encyclopedia
Search

Mars trojan

From Wikipedia, the free encyclopedia
Celestial bodies that share the orbit of Mars
TheL5 group (shown in green) and theL4 group (light blue) ofMars andJupitertrojan asteroids shown along with the orbits of Jupiter and the inner planets. Mars is shown in red. The outer orbit is that of Jupiter.
Animation of 1999 UJ7 relative to Sun and Mars 1600-2500
   Sun ·   1999 UJ7 ·   Mars
Animation of 2007 NS2 relative to Sun and Mars 1600-2500
   Sun ·   2007 NS2 ·   Mars

TheMars trojans are a group oftrojan objects that share theorbit of theplanetMars around theSun. They can be found around the twoLagrangian points 60° ahead of and behind Mars. The origin of the Mars trojans is not well understood. One theory suggests that they were primordial objects left over from the formation of Mars that were captured in its Lagrangian points as theSolar System was forming. However, spectral studies of the Mars trojans indicate this may not be the case.[1][2] Another explanation involves asteroids chaotically wandering into theMars Lagrangian points later in the Solar System's formation. This is also questionable considering the short dynamical lifetimes of these objects.[3][4] The spectra of Eureka and two other Mars trojans indicates anolivine-rich composition.[5] Since olivine-rich objects are rare in the asteroid belt it has been suggested that some of the Mars trojans are captured debris from a large orbit-altering impact on Mars when it encountered a planetary embryo.[6][3]

Presently, this group contains 17 asteroids confirmed to be stable Mars trojans by long-term numerical simulations but only nine of them are accepted by theMinor Planet Center.[7][3][4][8][9][10][11]

Due to close orbital similarities, most of the smaller members of the L5 group are hypothesized to be fragments ofEureka that were detached after theYORP effect accelerated Eureka's rotational period to the present 2.69 hours. The L4 trojan1999 UJ7 has a much longer rotational period of ~50 h, apparently due to a chaotic rotation that prevents YORP spinup.[12] The spectrum of 121514 show a certain resemblance to that of 2023 FW14 and a common origin cannot be discarded.[13] The spectra of 121514 and 2023 FW14 are very different from those of the Eureka asteroid family members.

List of Mars trojans
DesignationCloudSemimajor axis
(AU)
Perihelion
(AU)
EccentricityInclination
(°)
(H)Diameter
(m)
5261 EurekaL51.523561.424770.0648420.282016.131880±230
(101429) 1998 VF31L51.524291.371500.1002431.298717.261210+890
−350
(121514) 1999 UJ7L41.524551.464910.0391216.749317.192450±490
(311999) 2007 NS2L51.523791.441550.0539718.619418.18790+580
−230
(385250) 2001 DH47L51.523851.471110.0346124.400618.89570+420
−170
2009 SEL51.524511.425240.0651220.626319.9360+260
−110
2011 SL25L51.523911.349380.1145321.495319.5430+320
−120
2011 SP189L51.523861.462470.0402919.899420.9230+160
−70
2011 SC191L51.523901.456780.0440518.745119.4450+330
−130
2011 UN63L51.523781.425210.0646920.363519.7390+290
−110
2011 UB256L51.523701.415500.0710124.302319.9360+260
−110
2016 AA165L51.522991.386500.0896218.720220.39290+210
−90
2016 CP31L51.523651.434250.0586723.131419.4450+330
−130
2018 EC4L51.523651.431380.0605621.836220.0340+250
−100
2018 FC4L51.523881.497810.0171122.146621.2200+140
−60
2018 FM29L51.523911.451960.0472221.500421.11210+150
−60
2023 FW14L41.523771.282840.1581113.2727121.59318+493
−199

See also

[edit]

References

[edit]
  1. ^Rivkin, Andrew; Trilling, David; Thomas, Cristina; DeMeo, Fancesca; Spahr, Timoth; Binzel, Richard (2007). "Composition of the L5 Mars Trojans: Neighbors, not siblings".Icarus.192 (2):434–441.arXiv:0709.1925.Bibcode:2007Icar..192..434R.doi:10.1016/j.icarus.2007.06.026.S2CID 15118710.
  2. ^Trilling, David; Rivking, Andrew; Stansberry, John; Spahr, Timothy; Crudo, Richard; Davies, John (2007). "Albedos and diameters of three Mars Trojan asteroids".Icarus.192 (2):442–447.arXiv:0709.1921.Bibcode:2007Icar..192..442T.doi:10.1016/j.icarus.2007.08.002.S2CID 16618044.
  3. ^abcScholl, H.; Marzari, F.; Tricarico, P. (2005). "Dynamics of Mars Trojans".Icarus.175 (2):397–408.Bibcode:2005Icar..175..397S.doi:10.1016/j.icarus.2005.01.018.
  4. ^abSchwarz, R.; Dvorak, R. (2012). "Trojan capture by terrestrial planets".Celestial Mechanics and Dynamical Astronomy.113 (1):23–34.arXiv:1611.07413.Bibcode:2012CeMDA.113...23S.doi:10.1007/s10569-012-9404-4.S2CID 254375599.
  5. ^Borisov, G.; Christou, A.; Bagnulo, S.; Cellino, A.; Kwiatkowski, T.; Dell'Oro, A. (2017)."he olivine-dominated composition of the Eureka family of Mars Trojan asteroids".Monthly Notices of the Royal Astronomical Society.466 (1):489–495.arXiv:1701.07725.Bibcode:2017MNRAS.466..489B.doi:10.1093/mnras/stw3075.
  6. ^Polishook, D.; Jacobson, S. A.; Morbidelli, A.; Aharonson, O. (2017). "A Martian origin for the Mars Trojan asteroids".Nature Astronomy.1 (8): 0179.arXiv:1710.00024.Bibcode:2017NatAs...1E.179P.doi:10.1038/s41550-017-0179.S2CID 119432820.
  7. ^"List Of Martian Trojans".Minor Planet Center. Retrieved2021-01-12.
  8. ^de la Fuente Marcos, Carlos; de la Fuente Marcos, Raúl (April 2013)."Three new stable L5 Mars Trojans".Monthly Notices of the Royal Astronomical Society: Letters.432 (1):L31 –L35.arXiv:1303.0124.Bibcode:2013MNRAS.432L..31D.doi:10.1093/mnrasl/slt028.
  9. ^Christou, A. A. (2013). "Orbital clustering of Martian Trojans: An asteroid family in the inner solar system?".Icarus.224 (1):144–153.arXiv:1303.0420.Bibcode:2013Icar..224..144C.doi:10.1016/j.icarus.2013.02.013.S2CID 119186791.
  10. ^Christou, Apostolos A.; Borisov, Galin; Dell'Oro, Aldo; Cellino, Alberto; Devogèle, Maxime (January 2021). "Composition and origin of L5 Trojan asteroids of Mars: Insights from spectroscopy".Icarus.354 (1): 113994 (22 pages).arXiv:2010.10947.Bibcode:2021Icar..35413994C.doi:10.1016/j.icarus.2020.113994.S2CID 224814529.
  11. ^de la Fuente Marcos, Carlos; de la Fuente Marcos, Raúl (March 2021)."Using Mars co-orbitals to estimate the importance of rotation-induced YORP break-up events in Earth co-orbital space".Monthly Notices of the Royal Astronomical Society.501 (4):6007–6025.arXiv:2101.02563.Bibcode:2021MNRAS.501.6007D.doi:10.1093/mnras/stab062.
  12. ^Lovett, R. (2017-10-20). "Sun's light touch explains asteroids flying in formation behind Mars".Science.doi:10.1126/science.aar2794.
  13. ^de la Fuente Marcos, Raúl; de León, Julia; de la Fuente Marcos, Carlos; Alarcon, Miguel R.; Licandro, Javier; Serra-Ricart, Miquel; Geier, Stefan; Cabrera-Lavers, Antonio (2024-03-21)."Dynamics of 2023 FW14, the second L4 Mars trojan, and a physical characterization using the 10.4 m Gran Telescopio Canarias".Astronomy & Astrophysics, Letters to the Editor.683 (1): L14 (6 pages).arXiv:2403.04061.Bibcode:2024A&A...683L..14D.doi:10.1051/0004-6361/202449688.{{cite journal}}: CS1 maint: date and year (link)
Main
Distribution
Classification
Orbital
Spectral
Tholen
SMASS
Exploration
Lists
Related
Minor planets
Asteroid
Distant minor planet
Comets
Other
Geography
Atmosphere
Regions
Physical
features
Geology
History
Astronomy
Moons
Transits
Asteroids
Comets
General
Exploration
Concepts
Missions
Advocacy
Related
Portal:
Retrieved from "https://en.wikipedia.org/w/index.php?title=Mars_trojan&oldid=1277409034"
Categories:
Hidden categories:

[8]ページ先頭

©2009-2025 Movatter.jp